Journal of Environmental Biology Alpine Marmot Populations After

Total Page:16

File Type:pdf, Size:1020Kb

Journal of Environmental Biology Alpine Marmot Populations After « Journal Home page : www.jeb.co.in E-mail : [email protected] OriginalTM Research Journal of Environmental Biology TM PDlagiarism etector JEB ISSN: 0254-8704 (Print) DOI : http://doi.org/10.22438/jeb/38/5/MRN-381 ISSN: 2394-0379 (Online) CODEN: JEBIDP Alpine marmot populations after four decades of living in the glacial areas of the Făgăraş, Rodna and Retezat Mountains, Romania Abstract Authors Info Aim : To highlight the situation of the alpine marmot (Marmota marmota) after four decades of colonisation S. Geacu and M. Dumitraşcu* in three mountain ranges of Romania: the Făgăraş, Rodna and Retezat. Department of Physical Geography, Institute of Geography, Methodology : To reach this target, summer field investigations have been conducted in various areas of Romanian Academy, 12 Dimitrie the three mountain ranges, and in the archives of central and local forest and hunting administrative units, Racoviţă Street, 023993, Sector 2, with a view to identify the data needed to establish the dynamics of these populations. Bucharest, Romania Results : A synthesis study has been made to point out the population dynamics of this rodent (Sciuridae Family), the connection between populationsCopy and the geographical conditions in the glacial areas of the three mountain groups of the Eastern and Southern Carpathians. Interpretation : A typical rodent of the Alpine regions, the alpine marmot s are perfectly integrated in thair new habitats with several colonies of these populations in each mountain group. At the same time, the species has extended its areas by up to 20 km. *Corresponding Author Email : [email protected] Key words Alpine marmot, Făgăraş mountain, Retezat mountain, Rodna mountain Online Publication Info Paper received : 10.06.2016 Revised received : 29.09.2016 Re-revised received : 13.02.2017 Accepted : 28.03.2017 © Triveni Enterprises, Lucknow (India) Journal of Environmental Biology September 2017 Vol. 38 703-711 704 S. Geacu and M. Dumitraşcu Introduction The current paper focuses on the analysis of the spatial and temporal dynamics of Marmota marmota in the three A rodent mammal, Marmota marmota lives in the alpine aforementioned areas in close connection with their habitat habitats of the highest mountains in Europe (Pyrenees, Alps and requirements and the conservation regime. The study was carried Carpathians). The mammal belongs to Order : Rodentia Bodwich, out for the past four decades, a period which followed species' 1821; Family : Sciuridae Gray, 1821 and Genus : Marmota introduction or re-introduction in the fauna of the Romanian Blumenbach, 1779 (Wilson and Reeder, 1993). Carpathians using the data provided by the Romanian Forest Divisions which overlapped Rodna, Făgăraş and Retezat Mountains. Studies performed in the Tatra Mountains (Bačkor 2009), Rodna Mountains (Szabo, 2010), the French and Italian Alps Study area : The present study was carried out in three of the (Allainé et al., 1994; Borgo, 2003) and the Pyrenees (Herrero et highest Romanian Carpathians Mountains: the Făgăraş and al., 1994) revealed significant information on species current Retezat in the Southern Carpathians and the Rodna Mountains distribution, dynamics and habitat requirements in the in the Eastern Carpathians (Fig. 1B), all being built mountaineous areas of Europe. predominantly of crystalline schists (Niculescu and Badea, 2006). They have the most impressive glacial relief (glacial In Romania, Marmota marmota was introduced to the cirques and valleys) of all mountain ranges in this country tallest Romanian Carpathians, which is, Făgăraş and Retezat (Niculescu et al., 1973). Springs on slopes and glacial lakes (Southern Carpathians) and Rodna (Eastern Carpathians) represent water sources for the alpine marmot. (Almăşan, 1981; Geacu, 2006). Materials and Methods As herbaceous species, the alpine marmot feeds on the short plants (Carex curvula, Juncus trifidus, Agrostis rupestris, At the time the first alpine marmots were brought into Festuca airoides, Nardus stricta, Sesleria tenuifolia and Poa Romania, the researches were focused primarily on identifying alpina) that grow in alpine meadows and are well-adapted to the first documents issued by various forestry and cynegetic cold and strong winds. It also eats the lickhens that gnaw on institutions. Later on, studies performed in the selected case- rocks, e.g. Cetraria islandica or Cladonia rangiferina, and grows studies aimed at establishing the population dynamics and at the bark of dwarf bushes such as Loiseleuria procumbens of species Copyhabitat characteristics. The assessment of long-term the alpine zone. The alpine marmot also eat the fruits of some dynamics relied on the data recorded by the rangers of the Forest species like Vaccinium myrtillus and Vaccinium vitis-idaea. Divisions in the analysed mountain areas. Thereby, in 2011 and Alpine marmots are fond of sunny slopes and if nothing disturbs 2012 the authors carried out direct field observations in the areas them, they may bathe in the sun for hours on end. Between where alpine marmots used to live during summertime. Based on October to April, the animal hibernates, the entrance to the the visual observations (using binoculars) conducted during the galleries being closed with stones, grass and earth (Năidăşan, field surveys, the authors were able to map several alpine marmot 2000). Moreover, some studies refer to the impact of global habitats and movement routes. climate changes on the shortening of the hibernation period (Inouye et al., 2000, Dolenec and Dolenec, 2011). Results and Discussion It has been considered that the alpine marmot inhabited The Făgăraş Mountains : The Făgăraş Mountains covers the highest areas of Rodna, Făgăraş and Retezat Mountains 2 during the 19th century (Bielz, 1888; Csato, 1867), whereto it has approximately 1,500 km with a dominant altitude of 2,400- been disappeared between 1890 and 1900 (Călinescu, 1931; 2,500 m a.s.l., favouring the development of alpine and Filipaşcu, 1969). Species' existence in Romania was contested subalpine levels. Likewise, the massif features a significant by Rosetti-Bălănescu, (1973) by arguing the absence of any glacial relief inherited also from periglacial processes of reference to this species in the Romanian folklore or the toponimy extensive spatial dynamic (Voiculescu, 2002; Voiculescu and of this space (Benedek, 2014). However, a proposal for having the Ardelean, 2012). It also preserves the widest glacial area in species reintroduced in Romania dates back to 1949, but it was Romania, especially on the main summit which is about 70 km only in 1965, when Almăşan stressed upon the Online« need to begin long from west to east, with maximum elevation in the country: acting to this end as soon as possible » (p. 12), that their future the Moldoveanu (2,544 m a.s.l.) and the Negoiu (2,535 m a.s.l.) habitat (Făgăraş and Retezat Mountains) was being designated peaks. Here, one may see complex glacial cirques, up to 8 km- (Almăşan, 1965). The first 50 alpine marmot individuals were long glacial valleys and 25 glacial lakes (e.g. Lacul Doamnei – brought into Romania in 1973, having been captured in the Alps. Lake of the Lady 0.5 ha and Podrăgel Lake – 0.7 ha lie at 1,860 Out of the 33 animals caught in the Vanoise National Park m a.s.l. and 2,030 m a.s.l., respectively) (Niculescu, 1973; (France), 21 were released in the Făgăraş Mountains and 12 in Velcea and Popova, 1987) (Fig. 2). the Rodna Mountains. A number of 17 individuals came from Salzburg region (Austria) and were released in the Retezat At Bâlea Lac weather station (2,038 m a.s.l.), the mean Mountains (Fig. 1A, Fig. 1B). annual air temperature is only 0.2°C, with a maximum of 8.8°C) in Journal of Environmental Biology, September 2017 Alpine marmot in Romanian Carpathians 705 August and a minimum of -8.4°C in February (Fig. 3A) ; the mean Outstanding among the 58 glacial lakes are Bucura (10 annual rainfall reaches 1215 mm (Sandu et al., 2008). The ha), Zănoaga (29 m, the deepest glacial lake in Romania) and dominant winds blow from the north (21.1%) (Voiculescu, 2002). Gemenele (2.5 ha) (Pişota, 1971; Gâştescu, 1971; Popovici, The annual number of days with snow cover is 150, except for the 1993). At Ţarcu weather station (2,180 m a.s.l), situated in the summer and the first half of winter when no such days are neighbouring mountain sector, the mean annual air temperature registered (Fig. 3B). is negative (-0.6°C), with a maximum value in August (7.7°C) and a minimum in February (-8.6°C) (Fig. 5A). The mean annual The habitat conditions of the upper Făgăraş Mountains precipitation sums up to 939.4 mm. The dominant wind blows are favourable to the alpine marmot. The species was introduced from the north (21.5%) and the snow cover may appear in the first in the area in July 1973, when 21 alpine marmots were brought decade of September and it lasts until July or August (Fig. 5B). from the French Alps and were released in the glacial cirque at the The annual number of days with snow cover was 190 days on sources of the Arpăşel Valley (northern slope of Făgăraş average (Dragne et al., 2004). Mountains, Sibiu County). Here, the staff of the Arpaş Forest Range built man-made galleries in order to host them and The upper part of the Retezat Mountains was established prohibited the grazing of farm animals. This action enjoyed the in 1935 as the first national park in Romania (10,000 ha). support of the Inspection for the Economy of Hunting of the Currently, the surface of this protected area has been extended to Ministry of Forest Economy and Building Materials (Almășan, 38,047 ha, of which 1,630 ha is covered by Gemenele Scientific 1981). At the beginning, the alpine marmots settled at 1,900- Reserve.
Recommended publications
  • Guidelines for Wildlife and Traffic in the Carpathians
    Wildlife and Traffic in the Carpathians Guidelines how to minimize the impact of transport infrastructure development on nature in the Carpathian countries Wildlife and Traffic in the Carpathians Guidelines how to minimize the impact of transport infrastructure development on nature in the Carpathian countries Part of Output 3.2 Planning Toolkit TRANSGREEN Project “Integrated Transport and Green Infrastructure Planning in the Danube-Carpathian Region for the Benefit of People and Nature” Danube Transnational Programme, DTP1-187-3.1 April 2019 Project co-funded by the European Regional Development Fund (ERDF) www.interreg-danube.eu/transgreen Authors Václav Hlaváč (Nature Conservation Agency of the Czech Republic, Member of the Carpathian Convention Work- ing Group for Sustainable Transport, co-author of “COST 341 Habitat Fragmentation due to Trans- portation Infrastructure, Wildlife and Traffic, A European Handbook for Identifying Conflicts and Designing Solutions” and “On the permeability of roads for wildlife: a handbook, 2002”) Petr Anděl (Consultant, EVERNIA s.r.o. Liberec, Czech Republic, co-author of “On the permeability of roads for wildlife: a handbook, 2002”) Jitka Matoušová (Nature Conservation Agency of the Czech Republic) Ivo Dostál (Transport Research Centre, Czech Republic) Martin Strnad (Nature Conservation Agency of the Czech Republic, specialist in ecological connectivity) Contributors Andriy-Taras Bashta (Biologist, Institute of Ecology of the Carpathians, National Academy of Science in Ukraine) Katarína Gáliková (National
    [Show full text]
  • The Catalogue of the Freshwater Crayfish (Crustacea: Decapoda: Astacidae) from Romania Preserved in “Grigore Antipa” National Museum of Natural History of Bucharest
    Travaux du Muséum National d’Histoire Naturelle © Décembre Vol. LIII pp. 115–123 «Grigore Antipa» 2010 DOI: 10.2478/v10191-010-0008-5 THE CATALOGUE OF THE FRESHWATER CRAYFISH (CRUSTACEA: DECAPODA: ASTACIDAE) FROM ROMANIA PRESERVED IN “GRIGORE ANTIPA” NATIONAL MUSEUM OF NATURAL HISTORY OF BUCHAREST IORGU PETRESCU, ANA-MARIA PETRESCU Abstract. The largest collection of freshwater crayfish of Romania is preserved in “Grigore Antipa” National Museum of Natural History of Bucharest. The collection consists of 426 specimens of Astacus astacus, A. leptodactylus and Austropotamobius torrentium. Résumé. La plus grande collection d’écrevisses de Roumanie se trouve au Muséum National d’Histoire Naturelle «Grigore Antipa» de Bucarest. Elle comprend 426 exemplaires appartenant à deux genres et trois espèces, Astacus astacus, A. leptodactylus et Austropotamobius torrentium. Key words: Astacidae, Romania, museum collection, catalogue. INTRODUCTION The first paper dealing with the freshwater crayfish of Romania is that of Cosmovici, published in 1901 (Bãcescu, 1967) in which it is about the freshwater crayfish from the surroundings of Iaºi. The second one, much complex, is that of Scriban (1908), who reports Austropotamobius torrentium for the first time, from Racovãþ, Bahna basin (Mehedinþi county). Also Scriban made the first comment on the morphology and distribution of the species Astacus astacus, A. leptodactylus and Austropotamobius torrentium, mentioning their distinctive features. Also, he published the first drawings of these species (cephalothorax). Entz (1912) dedicated a large study to the crayfish of Hungary, where data on the crayfish of Transylvania are included. Probably it is the amplest paper dedicated to the crayfish of the Romanian fauna from the beginning of the last century, with numerous data on the outer morphology, distinctive features between species, with more detailed figures and with the very first morphometric measures, and also with much detailed data on the distribution in Transylvania.
    [Show full text]
  • Endemic Macrolepidoptera Subspecies in the Natural History Museum Collections from Sibiu (Romania)
    Travaux du Muséum National d’Histoire Naturelle © 31 août «Grigore Antipa» Vol. LVI (1) pp. 65–80 2013 DOI: 10.2478/travmu-2013-0005 ENDEMIC MACROLEPIDOPTERA SUBSPECIES IN THE NATURAL HISTORY MUSEUM COLLECTIONS FROM SIBIU (ROMANIA) SERGIU-CORNEL TÖRÖK, GABRIELA CUZEPAN Abstract. The paper presents data regarding endemic Macrolepidoptera subspecies preserved in the Entomological Collections of Natural History Museum from Sibiu. 22 endemic subspecies are recorded and represented by 382 specimens in the Entomological Collection. Most of the specimens have been collected from mountain habitats, especially from Southern and Western Carpathians. The results of this paper contribute to the improvement of the existing data concerning the distribution and outline the areas of Macrolepidoptera’s endemism in Romania. Résumé. Le document présente des données concernant les sous-espèces endémiques des Macrolépidoptères conservées dans les collections entomologiques du Musée d’Histoire Naturelle de Sibiu. 22 sous-espèces endémiques sont enregistrées et représentées par 382 spécimens dans la collection entomologique. La plupart des spécimens ont été recueillis dans les habitats de montagne, en particulier du Sud et l’Ouest des Carpates. Les résultats de cette étude contribuent à compléter les données existantes concernant la distribution et de définir les zones d’endémisme des Macrolépidoptères en Roumanie. Key words: Macrolepidoptera, endemic taxa, geographic distribution, museum collections. INTRODUCTION In this paper, the authors wish to present the endemic taxa from the Natural History Museum from Sibiu. The term endemic is used for taxa that are unique to a geographic location. This geographic location can be either relatively large or very small (Gaston & Spicer, 1998; Kenyeres et al., 2009).
    [Show full text]
  • Intensified Grazing Affects Endemic Plant and Gastropod
    Biologia, Bratislava, 62/4: 438—445, 2007 Section Zoology DOI: 10.2478/s11756-007-0086-4 Intensified grazing affects endemic plant and gastropod diversity in alpine grasslands of the Southern Carpathian mountains (Romania) Bruno Baur1,CristinaCremene1,2, Gheorghe Groza3,AnatoliA.Schileyko4, Anette Baur1 & Andreas Erhardt1 1Section of Conservation Biology, Department of Environmental Sciences, University of Basel, St. Johanns-Vorstadt 10, CH-4056 Basel, Switzerland; e-mail: [email protected] 2Faculty of Biology and Geology, Babes-Bolyai University, Str. Clinicilor 5–7, 400006 Cluj-Napoca, Romania 3Department of Botany, University of Agricultural Sciences and Veterinary Medicine, Calea Manastur 3–5, 400372 Cluj- Napoca, Romania 4A.N. Severtzov Institute of Problems of Evolution and Ecology of the Russian Academy of Sciences, Leninski Prospect 33, 119017 Moscow, Russia Abstract: Alpine grasslands in the Southern Carpathian Mts, Romania, harbour an extraordinarily high diversity of plants and invertebrates, including Carpathic endemics. In the past decades, intensive sheep grazing has caused a dramatic de- crease in biodiversity and even led to eroded soils at many places in the Carpathians. Because of limited food resources, sheep are increasingly forced to graze on steep slopes, which were formerly not grazed by livestock and are considered as local biodiversity hotspots. We examined species richness, abundance and number of endemic vascular plants and terres- trial gastropods on steep slopes that were either grazed by sheep or ungrazed by livestock in two areas of the Southern Carpathians. On calcareous soils in the Bucegi Mts, a total of 177 vascular plant and 19 gastropod species were recorded. Twelve plant species (6.8%) and three gastropod species (15.8%) were endemic to the Carpathians.
    [Show full text]
  • Background and Introduction
    Chapter One: Background and Introduction Chapter One Background and Introduction title chapter page 17 © Libor Vojtíšek, Ján Lacika, Jan W. Jongepier, Florentina Pop CHAPTER?INDD Chapter One: Background and Introduction he Carpathian Mountains encompass Their total length of 1,500 km is greater than that many unique landscapes, and natural and of the Alps at 1,000 km, the Dinaric Alps at 800 Tcultural sites, in an expression of both km and the Pyrenees at 500 km (Dragomirescu geographical diversity and a distinctive regional 1987). The Carpathians’ average altitude, how- evolution of human-environment relations over ever, of approximately 850 m. is lower compared time. In this KEO Report, the “Carpathian to 1,350 m. in the Alps. The northwestern and Region” is defined as the Carpathian Mountains southern parts, with heights over 2,000 m., are and their surrounding areas. The box below the highest and most massive, reaching their offers a full explanation of the different delimi- greatest elevation at Slovakia’s Gerlachovsky tations or boundaries of the Carpathian Mountain Peak (2,655 m.). region and how the chain itself and surrounding areas relate to each other. Stretching like an arc across Central Europe, they span seven countries starting from the The Carpathian Mountains are the largest, Czech Republic in the northwest, then running longest and most twisted and fragmented moun- east and southwards through Slovakia, Poland, tain chain in Europe. Their total surface area is Hungary, Ukraine and Romania, and finally 161,805 sq km1, far greater than that of the Alps Serbia in the Carpathians’ extreme southern at 140,000 sq km.
    [Show full text]
  • Harttimo 1.Pdf
    Beyond the River, under the Eye of Rome Ethnographic Landscapes, Imperial Frontiers, and the Shaping of a Danubian Borderland by Timothy Campbell Hart A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Greek and Roman History) in the University of Michigan 2017 Doctoral Committee: Professor David S. Potter, Co-Chair Professor Emeritus Raymond H. Van Dam, Co-Chair Assistant Professor Ian David Fielding Professor Christopher John Ratté © Timothy Campbell Hart [email protected] ORCID iD: 0000-0002-8640-131X For my family ii ACKNOWLEDGEMENTS Developing and writing a dissertation can, at times, seem like a solo battle, but in my case, at least, this was far from the truth. I could not have completed this project without the advice and support of many individuals, most crucially, my dissertation co-chairs David S. Potter, and Raymond Van Dam. Ray saw some glimmer of potential in me and worked to foster it from the moment I arrived at Michigan. I am truly thankful for his support throughout the years and constant advice on both academic and institutional matters. In particular, our conversations about demographics and the movement of people in the ancient world were crucial to the genesis of this project. Throughout the writing process, Ray’s firm encouragement towards clarity of argument and style, while not always what I wanted to hear, have done much to make this a stronger dissertation. David Potter has provided me with a lofty academic model towards which to strive. I admire the breadth and depth of his scholarship; working and teaching with him have shown me much worth emulating.
    [Show full text]
  • Western Carpathians, Poland)
    Geological Quarterly, 2006, 50 (1): 169–194 Late Jurassic-Miocene evolution of the Outer Carpathian fold-and-thrust belt and its foredeep basin (Western Carpathians, Poland) Nestor OSZCZYPKO Oszczypko N. (2006) — Late Jurassic-Miocene evolution of the Outer Carpathian fold-and-thrust belt and its foredeep basin (Western Carpathians, Poland). Geol. Quart., 50 (1): 169–194. Warszawa. The Outer Carpathian Basin domain developed in its initial stage as a Jurassic-Early Cretaceous rifted passive margin that faced the east- ern parts of the oceanic Alpine Tethys. Following closure of this oceanic basin during the Late Cretaceous and collision of the Inner Western Carpathian orogenic wedge with the Outer Carpathian passive margin at the Cretaceous-Paleocene transition, the Outer Carpathian Basin domain was transformed into a foreland basin that was progressively scooped out by nappes and thrust sheets. In the pre- and syn-orogenic evolution of the Outer Carpathian basins the following prominent periods can be distinguished: (1) Middle Juras- sic-Early Cretaceous syn-rift opening of basins followed by Early Cretaceous post-rift thermal subsidence, (2) latest Creta- ceous-Paleocene syn-collisional inversion, (3) Late Paleocene to Middle Eocene flexural subsidence and (4) Late Eocene-Early Miocene synorogenic closure of the basins. In the Outer Carpathian domain driving forces of tectonic subsidence were syn-rift and thermal post-rift processes, as well as tectonic loads related to the emplacement of nappes and slab-pull. Similar to other orogenic belts, folding of the Outer Carpathians commenced in their internal parts and progressed in time towards the continental foreland. This process was initi- ated at the end of the Paleocene at the Pieniny Klippen Belt/Magura Basin boundary and was completed during early Burdigalian in the northern part of the Krosno Flysch Basin.
    [Show full text]
  • Európa Regionális Földrajza
    Európa regionális földrajza Természetföldrajz Gábris, Gyula Horváth, Erzsébet Horváth, Gergely Kéri, András Móga, János Nagy, Balázs Nemerkényi, Antal Pavlics, Károlyné Simon, Dénes Telbisz, Tamás Created by XMLmind XSL-FO Converter. Európa regionális földrajza: Természetföldrajz írta Gábris, Gyula, Horváth, Erzsébet, Horváth, Gergely, Kéri, András, Móga, János, Nagy, Balázs, Nemerkényi, Antal, Pavlics, Károlyné, Simon, Dénes, és Telbisz, Tamás Publication date 2014 Szerzői jog © 2014 ELTE Eötvös Kiadó Created by XMLmind XSL-FO Converter. Tartalom Előszó ................................................................................................................................................ vi 1. Európa természeti viszonyai ........................................................................................................... 1 1. 1. Kedvező földrajzi helyzet .................................................................................................. 1 2. 2. Kétarcú domborzati kép .................................................................................................... 2 3. 3. Európa születése ................................................................................................................ 2 4. 4. „Távvezérelt” éghajlat ....................................................................................................... 7 5. 5. A vízrajz a domborzat és az éghajlat tükre ...................................................................... 17 6. 6. A tundráktól a sztyeppekig .............................................................................................
    [Show full text]
  • Deglaciation Constraints in the Parang Mountains, Southern Romania
    Quaternary International xxx (2015) 1e12 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Deglaciation constraints in the Parang^ Mountains, Southern Romania, using surface exposure dating * D.M. Gheorghiu a, , M. Hosu b, C. Corpade b,S.Xuc a CIAF- NERC, Scottish Universities Environmental Research Centre, East Kilbride G75 0QF, UK b Faculty of Geography, Babes¸ -Bolyai University, Str.Clinicilor Nr. 5-7, 400006, Romania c AMS, Scottish Universities Environmental Research Centre, East Kilbride G75 0QF, UK article info abstract Article history: Cosmogenic nuclide surface exposure ages have been widely used to constrain glacial chronologies in the Available online xxx European regions. This paper brings new evidence that the Romanian Carpathians sheltered mountain glaciers in their upper valleys and cirques until the end of the last glaciation. Twenty-four 10Be surface Keywords: exposure ages were obtained from boulders on moraine crests in the central area of the Parang^ Glaciers Mountains, Southern Carpathians. Exposure ages were used to constrain the timing of the deglaciation Glacial geomorphology events during the Late Glacial. The lowest boulders yielded an age of 13.0 ± 1.1 (1766 m) and final Deglaciation deglaciation occurred at 10.2 ± 0.9 ka (2055 m). Timing of the Late Glacial events and complete degla- Surface exposure ages fi Parang^ Mountains ciation reported in this study are consistent with, and con rm, previously reported ages of deglaciation Romania within the Carpathian and surrounding European region. © 2015 Elsevier Ltd and INQUA. This is an open access article under the CC BY license (http:// creativecommons.org/licenses/by/4.0/).
    [Show full text]
  • Forest Stands from Accumulation and Natural Lakes Slopes from the Southern Carpathians
    https://doi.org/10.15551/pesd2020141016 PESD, VOL. 14, no. 1, 2020 FOREST STANDS FROM ACCUMULATION AND NATURAL LAKES SLOPES FROM THE SOUTHERN CARPATHIANS Dincă Lucian1, Voichița Timiș-Gânsac2, Breabăn Iuliana Gabriela3 Keywords: lakes, forests, exposition, field inclination, forest soils. Abstract. The Southern Carpathians are situated in the central part of Romania, between Prahova Valley and the Danube, being the highest and most massive mountains from the Romanian Carpahtians. The relief and vegetation are similar to the Alps. These mountains conserve the most representative glaciar relief from Romania, with cuaternar glaciar tracks. Some of its peaks, namely Moldoveanu, Negoiu, Parângul Mare and Peleaga exceed 2500 m. From its total 217.889 ha occupied by forests with water protection functions, the forests located on lake slopes occupy 9.746 ha, namely 5%. The forests from this area are composed of spruce (Picea abies L.H. Karst) and beech (Fagus sylvatica L.), accompanied by other species such as birch (Alnus glutinosa, L., Gaertn.) and pine (Pinus sp.). From the point of view of the field’s orography, these forests are located on lands with an middle inclination on all exposition categories, but predominantly on the North-East, one at an average altitude of 1050 m. From the point of view of site conditions, the characteristic flora type is Asperula-Dentaria, while the main soils are dystric cambisol and eutric cambisol. 1. Introduction The Southern Carpathians are situated within Prahova Valley in the east, and Timiş-Cerna valleys in the west, Getic Subcarpathians and Mehedinți Plateau in the south and Transylvania’s basin in the north.
    [Show full text]
  • BESZÁMOLÓ a Magyar Földrajzi Társaság HEGYMÁSZÓ SZAKOSZTÁLYÁNAK 1978 Évi Működéséről
    BESZÁMOLÓ A Magyar Földrajzi Társaság HEGYMÁSZÓ SZAKOSZTÁLYÁNAK 1978 évi működéséről BUDAPEST 1979 Beszámoló Magyar Földrajzi Társaság HEGYMÁSZÓ SZAKOSZTÁLYÁNAK 1978 évi működéséről szeállitották: dr Dezsényi János szakosztályi elnök ifj. Kalmár László szakosztályi titkár Karlócai Miklós szakosztályi titkár Adler-Rácz József munkája a II. rész Józsa Sándor műszaki szerkesztő Arno Puskás, grafika Tálos Zoltán, foto PÉTERVÁRI- Q3 U-erdeygruz gyűjtemény ro B u d a p e s t 1979 ISBN 963 7321 25 S U M M A R Y Thö-S 1978 Report of the Mountain Climbing Section of the Hungár­ ián Geographical Society contains four parts. In the first part the pást events of the lastyear are discussed. - The predecessor of the Section, the Budapest University Tourist Club has been founded 7o years ago. - This year there were 11 lectures delivered by the members about the Eastern and Western Alps, the Dolomites, the Czech Sand-rocks, the High Tatras and the Southern Carpa- thians /the Fogaras Alps/. Three foreign lecturers were invited too;Ivan Gálfy from Slovakia reported on the Maka- lu /8481 m/ expedition of 1976, Prakash Bis Singh Tuladhar narrated about his native land Nepál, and Peter Baumgart- ner gave a lecture on the Spitzbergen. - A so-called Nestor-meeting was arranged where the 9 2 years old dr Barcza Ferenc was the senior. Moreover 12 climbers over 7o years made their appearance too. - Neidenbach Ákos led a climbing course of four theoretical and four practical lessons fór the juniors. The second part summarizes the high-mountain tours of the mem­ bers of the Section. Determined by the travel distances the main goal of the tours were the Carpathians.
    [Show full text]
  • Contribution to the Pseudoscorpion Fauna of Transylvania and the Eastern and Southern Carpathians, Romania (Arachnida: Pseudoscorpiones)
    NORTH-WESTERN JOURNAL OF ZOOLOGY 15 (2): 127-134 ©NWJZ, Oradea, Romania, 2019 Article No.: e181302 http://biozoojournals.ro/nwjz/index.html Contribution to the pseudoscorpion fauna of Transylvania and the Eastern and Southern Carpathians, Romania (Arachnida: Pseudoscorpiones) János NOVÁK1*, Daniel JABLONSKI2 and Jana CHRISTOPHORYOVÁ2 1. Department of Systematic Zoology and Ecology, Eötvös Loránd University, Pázmány Pétersétány 1/C, H-1117 Budapest, Hungary. 2. Department of Zoology, Faculty of Natural Sciences, Comenius University, Mlynská dolina, Ilkovičova 6, SK–842 15 Bratislava, Slovakia. *Corresponding author, J. Novák, E-mail: [email protected] Received: 03. February 2017 / Accepted: 12. November 2018 / Available online: 19. November 2018 / Printed: December 2019 Abstract. New records for the pseudoscorpion fauna of Transylvania and the Eastern and Southern Carpathians (Romania) are presented, based on material in the Hungarian Natural History Museum (HNHM) and the Bakony Museum of the HNHM, along with material collected by the authors. Eighteen species of five families are recorded; one of the species, Chthonius carinthiacus Beier, 1951, is new for the fauna of Romania. New data concerning the recently described Neobisium tothi Novák, 2017 are presented. The number of pseudoscorpion species recorded for Romania is raised to 77. Neobisium blothroides (Tömösváry, 1882) is removed from the fauna of Croatia. Keywords: Carpathians, new records, pseudoscorpions, Romania, Transylvania. Introduction ern Carpathians (Dumitresco & Orghidan 1969), with D. bal- canicus (Redikorzev, 1929). Gardini (2014) synonymised two Romania covers a great variety of geographical areas and species, Chthonius diophthalmus Daday, 1889, described from natural habitats, from the coasts of the Black Sea across the ‘Mehádia’ (southern Carpathians) (Daday 1889a), and C.
    [Show full text]